Dry Density of Solids Formula:
Definition: Dry Density of Solids is the mass of the solid particles per unit volume of the soil when all the pore spaces are filled with air.
Purpose: It's a fundamental property in soil mechanics used to evaluate soil compaction and quality.
The calculator uses the formula:
Where:
Explanation: The weight of solids is divided by the volume they occupy to determine the dry density.
Details: Dry density is crucial for determining soil compaction, bearing capacity, and settlement characteristics in geotechnical engineering.
Tips: Enter the weight of solids in kg, volume of solids in m³, and tolerance percentage (default ±5%). All values must be > 0.
Q1: What is a typical dry density range for soils?
A: It varies by soil type: sands (1.4-1.7 g/cm³), silts (1.3-1.6 g/cm³), clays (1.1-1.5 g/cm³).
Q2: Why include a tolerance percentage?
A: The tolerance accounts for measurement uncertainties and natural variations in soil properties.
Q3: How is this different from bulk density?
A: Dry density considers only solids, while bulk density includes pore spaces filled with air or water.
Q4: What units should I use?
A: The calculator uses kg for weight and m³ for volume, resulting in kg/m³ units for density.
Q5: How accurate are the results?
A: Accuracy depends on precise measurement of weight and volume. The tolerance range helps assess reliability.